Investigation of nonisothermal two-dimensional filtration in multylayer reservoir

IF 0.3 Q4 MECHANICS
D. Islamov, A. Ramazanov
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引用次数: 0

Abstract

The problem of an unsteady temperature field during two-dimensional fluid filtration in a multilayer reservoir is investigated taking into account the barothermal effect, radial and vertical permeability inhomogeneities. The results of comparing the analytical and numerical calculations of the temperature changes of the fluid flowing from the reservoir for two various models of reservoir heterogeneity are presented. From the obtained results it follows that 1. The presence of radial inhomogeneity of permeability in the near-well zone of the layered formation leads to fluid flows between the layers, which affects the temperature change rate of the liquid flowing from individual layers. 2. Non-stationary temperature profiles over the thickness of the layered formation at low inflow times contain information about the flows between the layers due to radial inhomogeneity in the near-well zone of the formation. 3. Flows between layers lead to large errors in solving the inverse problem of estimating the distribution of permeability in the reservoir based on non-stationary temperature data. 4. The presence of flows between the layers does not exclude the possibility of estimating the radius of the contamination zone. 5. To correctly account for the influence of flows between layers when calculating the nonstationary temperature in a layered formation with a disturbed near-well zone, it is necessary either to use a two-dimensional numerical model of non-isothermal filtration or to change the algorithm for correcting the layer’s flow rate for short and long inflow times in the onedimensional analytical model.
多层储层非等温二维过滤研究
考虑气压效应、径向和垂向渗透率的不均匀性,研究了多层储层二维流体过滤过程中的非定常温度场问题。对两种不同的储层非均质性模型进行了分析计算和数值计算,比较了两种模型下储层流出流体温度变化的计算结果。从得到的结果可以得出:1。层状地层近井区渗透率存在径向不均匀性,导致层间流体流动,影响了各层流出液体的温度变化率。2. 在低流入时间,层状地层厚度上的非平稳温度曲线包含了由于地层近井区径向不均匀性导致的层间流动信息。3.层间流动导致在求解基于非平稳温度数据的储层渗透率分布反演问题时误差较大。4. 层间流动的存在并不排除估计污染区半径的可能性。5. 在计算具有扰动近井带的层状地层的非平稳温度时,为了正确考虑层间流动的影响,有必要使用非等温过滤的二维数值模型,或者改变一维解析模型中用于校正短时间和长时间流入层流量的算法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.90
自引率
66.70%
发文量
0
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